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Nature Geoscience 1, 218 - 219 (2008)
doi:10.1038/ngeo167

Subject Category: Palaeoclimate and palaeoceanography

Palaeoclimate: Tree rings floating on ice cores

Paula J. Reimer1 & Konrad A. Hughen2

  1. The 14CHRONO Centre for Climate, the Environment & Chronology, School of Geography, Archaeology and Palaeoecology, Queen's University Belfast, Belfast, BT7 1NN, UK.
  2. Woods Hole Oceanographic Institution, Department of Marine Chemistry & Geochemistry, Woods Hole, Massachusetts 02543 USA.
    e-mail: p.j.reimer@qub.ac.uk


Because of difficulties in creating a radiocarbon calibration that covers the end of the last glaciation, defining the timing and duration of the Younger Dryas cold event has been a challenge. Linking related cosmogenic isotopes in tree rings and ice cores may provide new insights into abrupt climate changes.

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